Multiple Paleo-thermal Episodes in Mackenzie Corridor, Northwest Territory, Canada Revealed by Apatite Fission Track Analysis (AFTA): Implications for Hydrocarbon Prospectivity
Paul F. Green1, Ian R. Duddy1, Lee
Slind2, and Fred Rayer2
1 Geotrack International Pty Ltd,
Melbourne, Australia
2 Alconsult International Ltd,
Approximately 250 exploration wells have been drilled and in the
Mackenzie Corridor since the discovery of the Norman Wells oil field in 1920,
with relatively few successes. Likely reasons include lack of understanding of
potential sources, variation in maturation
histories across the region,
migration paths and availability of suitable traps at the time of migration,
across this large and structurally complex area. AFTA (Apatite Fission Track
Analysis) data in more than 20 wells from the region, integrated with organic
maturity (vitrinite reflectance) data, has revealed multiple paleo-thermal
episodes which exert significant control on
maturation
trends and hydrocarbon
prospectivity, resolving some of these uncertainties. Over much of the region,
Devonian units reached maximum maturities during the Jurassic, due to deep
burial and elevated basal heat flow. Cooling began some time between 190 and 170
Ma, due to reduction in heat flow plus exhumation. Subsequent Early Cretaceous
to Paleocene units were largely removed in two (or more) pulses of Cenozoic
exhumation beginning in the intervals 60 to 40 Ma (Paleocene-Eocene) and 15 to 5
Ma (Mid-Late Miocene). But in certain areas, Early Cretaceous-Paleocene
deposition was sufficient to heat underlying Devonian-Cambrian units to higher
temperatures than those reached during the Jurassic, restarting source rock
maturation
from Devonian source rocks and resulting in a second phase of
hydrocarbon generation during the Tertiary. We suggest that this style of
history characterises the Norman Wells Field, illustrating how the later timing
of
maturation
in such areas is more favourable for trapping and preservation of
hydrocarbon accumulations.
AAPG Search and Discovery Article #90039©2005 AAPG Calgary, Alberta, June 16-19, 2005